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Freshwater fluxes in the Weddell Gyre: Results from ?18O

Freshwater fluxes in the Weddell Gyre: Results from ?18O
Freshwater fluxes in the Weddell Gyre: Results from ?18O
Full-depth measurements of ?18O from 2008 to 2010 enclosing the Weddell Gyre in the Southern Ocean are used to investigate the regional freshwater budget. Using complementary salinity, nutrients and oxygen data, a four-component mass balance was applied to quantify the relative contributions of meteoric water (precipitation/glacial input), sea-ice melt and saline (oceanic) sources. Combination of freshwater fractions with velocity fields derived from a box inverse analysis enabled the estimation of gyre-scale budgets of both freshwater types, with deep water exports found to dominate the budget. Surface net sea-ice melt and meteoric contributions reach 1.8% and 3.2%, respectively, influenced by the summer sampling period, and ?1.7% and +1.7% at depth, indicative of a dominance of sea-ice production over melt and a sizable contribution of shelf waters to deep water mass formation. A net meteoric water export of approximately 37?mSv is determined, commensurate with local estimates of ice sheet outflow and precipitation, and the Weddell Gyre is estimated to be a region of net sea-ice production. These results constitute the first synoptic benchmarking of sea-ice and meteoric exports from the Weddell Gyre, against which future change associated with an accelerating hydrological cycle, ocean climate change and evolving Antarctic glacial mass balance can be determined.
Antarctic Bottom Water, freshwater cycle, oxygen isotope, dense water export
1364-503X
20130298
Brown, Peter J.
29f4e81e-e0c4-4147-984b-0215571fb2ca
Meredith, Michael
6b7bc238-08ea-44c6-99d8-180c732b512b
Jullion, Loic
de0b8cf4-1ce0-49ae-b83d-c310dc612810
Naveira Garabato, Alberto
97c0e923-f076-4b38-b89b-938e11cea7a6
Torres-Valdes, Sinhue
50398d55-4df9-4b9e-a431-16936300650c
Holland, Paul
bfa959f1-638a-4430-a95a-ace4dfa8a564
Leng, Melanie J.
71755042-2b5f-44a6-8420-019f13a4a946
Venables, Hugh
d4dcd535-4a30-4a49-8df8-ffa6b5ae1d47
Brown, Peter J.
29f4e81e-e0c4-4147-984b-0215571fb2ca
Meredith, Michael
6b7bc238-08ea-44c6-99d8-180c732b512b
Jullion, Loic
de0b8cf4-1ce0-49ae-b83d-c310dc612810
Naveira Garabato, Alberto
97c0e923-f076-4b38-b89b-938e11cea7a6
Torres-Valdes, Sinhue
50398d55-4df9-4b9e-a431-16936300650c
Holland, Paul
bfa959f1-638a-4430-a95a-ace4dfa8a564
Leng, Melanie J.
71755042-2b5f-44a6-8420-019f13a4a946
Venables, Hugh
d4dcd535-4a30-4a49-8df8-ffa6b5ae1d47

Brown, Peter J., Meredith, Michael, Jullion, Loic, Naveira Garabato, Alberto, Torres-Valdes, Sinhue, Holland, Paul, Leng, Melanie J. and Venables, Hugh (2014) Freshwater fluxes in the Weddell Gyre: Results from ?18O. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 372 (2019), 20130298. (doi:10.1098/rsta.2013.0298).

Record type: Article

Abstract

Full-depth measurements of ?18O from 2008 to 2010 enclosing the Weddell Gyre in the Southern Ocean are used to investigate the regional freshwater budget. Using complementary salinity, nutrients and oxygen data, a four-component mass balance was applied to quantify the relative contributions of meteoric water (precipitation/glacial input), sea-ice melt and saline (oceanic) sources. Combination of freshwater fractions with velocity fields derived from a box inverse analysis enabled the estimation of gyre-scale budgets of both freshwater types, with deep water exports found to dominate the budget. Surface net sea-ice melt and meteoric contributions reach 1.8% and 3.2%, respectively, influenced by the summer sampling period, and ?1.7% and +1.7% at depth, indicative of a dominance of sea-ice production over melt and a sizable contribution of shelf waters to deep water mass formation. A net meteoric water export of approximately 37?mSv is determined, commensurate with local estimates of ice sheet outflow and precipitation, and the Weddell Gyre is estimated to be a region of net sea-ice production. These results constitute the first synoptic benchmarking of sea-ice and meteoric exports from the Weddell Gyre, against which future change associated with an accelerating hydrological cycle, ocean climate change and evolving Antarctic glacial mass balance can be determined.

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More information

Published date: 2 January 2014
Keywords: Antarctic Bottom Water, freshwater cycle, oxygen isotope, dense water export
Organisations: Ocean Biochemistry & Ecosystems, Physical Oceanography

Identifiers

Local EPrints ID: 356911
URI: http://eprints.soton.ac.uk/id/eprint/356911
ISSN: 1364-503X
PURE UUID: 9ed9874b-d7ce-4db1-ac35-cef5e1401d4d
ORCID for Alberto Naveira Garabato: ORCID iD orcid.org/0000-0001-6071-605X

Catalogue record

Date deposited: 17 Sep 2013 08:57
Last modified: 15 Mar 2024 03:24

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Contributors

Author: Peter J. Brown
Author: Michael Meredith
Author: Loic Jullion
Author: Sinhue Torres-Valdes
Author: Paul Holland
Author: Melanie J. Leng
Author: Hugh Venables

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